A petroleum system encompasses a hydrocarbon source rock and all generated oil and gas accumulations and includes all the geologic elements and processes that are essential if an oil and gas deposit is to exist. Petroleum includes concentrated occurrences of any of the following substances: thermal and microbial natural gas found in conventional reservoirs as well as in gas hydrate, tight sandstone, fractured shale, and coal; and condensates, crude oils, heavy oils, and solid bitumen found in reservoirs in siliciclastic and carbonate rocks. System describes the interdependent geologic elements that create oil and gas accumulations. These elements include a petroleum source rock, migration path, reservoir rock, seal, and trap; and the geologic processes that create each of these basic elements. All these elements must be correctly placed in time and space so that organic matter included in a source rock can be converted into a petroleum deposit. A petroleum system exists wherever all the basic elements are known to occur or are thought to occur.Characteristics and Limits.-The stratigraphic, areal, and temporal extent of the petroleum system is specific. Stratigraphically, the system includes the following rock units: a petroleum source rock, rocks through which migration has occurred, a sealed reservoir rock (trap), and the rock overburden (time and temperature) required for maturity. The areal extent of the petroleum system is defined by a line that circumscribes the mature source rock and all oil and gas deposits, conventional and unconventional, originating from that source. Since microbial gas originates from immature source rocks, the gas deposits themselves or the geologic setting defines the extent of the system.The events of a petroleum system are defined by two periods of geologic time, the duration time and the preservation time. The duration is the time required to form a petroleum system. If the source rock is the first or oldest unit deposited and the overburden necessary to mature the source rock is the last or youngest element, then the age difference between the oldest and youngest element is the duration of the petroleum system. For example, a Devonian source rock (380-390 Ma) is buried by Pennsylvanian and Permian rocks (250-290 Ma) to maximum depth in the Late Permian(250 Ma); expulsion (primary migration) of hydrocarbons occurs during the Permian (250-275 Ma). These hydrocarbons migrate (secondary) and accumulate in reservoirs of Pennsylvanian age (300-315 Ma) and in traps that formed in the Late Pennsylvanian and Early Permian time (270-290 Ma). The duration of this petroleum system is 140 million years.Preservation time starts after migration (secondary) and accumulation are complete. If little or no tectonic activity occurs during the preservation time, accumulations will remain in their original position. Remigration (tertiary) happens during the preservation time if folding, faulting, uplift, or erosion occur. If all accumulations are destroyed during the preservation time, no record of th...